Influence of gas-particle partitioning on ammonia and nitric acid fluxes above a deciduous forest in the Midwestern USA

Kristina Hansen, Lise Lotte Sørensen, Karen E. Hornsby, Eva Boegh, Sara C. Pryor

Publikation: KonferencebidragKonferenceabstrakt til konferenceForskning

Resumé

Quantifying the atmosphere-biosphere exchange of reactive nitrogen gasses (including ammonia (NH3) and nitric acid (HNO3)) is crucial to assessing the impact of anthropogenic activities on natural and semi-natural ecosystems. However, measuring the deposition of reactive nitrogen is challenging due to bi-directionality of the flux, and the dynamics of the chemical gas/aerosol equilibrium of NH3 and HNO3 (or other atmospheric acids) with aerosol-phase ammonium (NH4+) and nitrate (NO3-). NH3 and HNO3 are both very reactive and typically exhibit higher deposition velocities than aerosol NH4+. Therefore, the phase partitioning between gas and aerosol phases can have a significant effect on local budgets and atmospheric transport distances (Nemitz et al., Atmos. Chem. Phys., 2004).

In this study, fluxes of NH3, HNO3 and carbon dioxide (CO2) along with size-resolved N-aerosol concentrations are measured above the deciduous forest, Morgan Monroe State Forest (MMSF) in south-central Indiana (39°53’N, 86°25’W) during a field campaign. Two relaxed eddy accumulation (REA) systems are used to measure fluxes and concentrations of NH3 and HNO3 at 44 m. The NH3 REA system operates based on wet effluent diffusion denuders with detection by florescence and half-hourly flux measurements are calculated. HNO3 REA system is based on gas capture on sodium chloride (NaCl) coated denuders with subsequent analysis by ion-chromatography, and the resulting fluxes have a resolution of 3-4 hours. CO2 fluxes are measured by eddy covariance using a closed-path Licor LI-7500, while two MSP MOUDI-110 impactors are used to measure the 24-hourly average inorganic and 48 hourly averaged organic ion concentrations in 11 size bins, respectively, just above the canopy level (28 m).

The results of this field campaign are used to quantify the fluxes of NH3, HNO3, CO2 to/from the forest during the transition towards senescence, and to investigate process-level controls (e.g. the role of phase partitioning) on the exchange of reactive nitrogen between the forest and the atmosphere.

OriginalsprogEngelsk
Publikationsdato2013
StatusUdgivet - 2013
BegivenhedAmerican Geophysical Union Fall Meeting 2013 - Moscone Center, San Francisco, USA
Varighed: 9 dec. 201313 dec. 2013
http://fallmeeting.agu.org/2013/

Konference

KonferenceAmerican Geophysical Union Fall Meeting 2013
LokationMoscone Center
LandUSA
BySan Francisco
Periode09/12/201313/12/2013
AndetAmerican Geophysical Union
Internetadresse

Emneord

  • atmosphere-biosphere exchange
  • fluxes
  • nitrogen
  • gas-particle partitioning
  • forest
  • relaxed eddy accummulation
  • eddy covariance

Citer dette

Hansen, K., Sørensen, L. L., Hornsby, K. E., Boegh, E., & Pryor, S. C. (2013). Influence of gas-particle partitioning on ammonia and nitric acid fluxes above a deciduous forest in the Midwestern USA. Abstract fra American Geophysical Union Fall Meeting 2013, San Francisco, USA.
Hansen, Kristina ; Sørensen, Lise Lotte ; Hornsby, Karen E. ; Boegh, Eva ; Pryor, Sara C. / Influence of gas-particle partitioning on ammonia and nitric acid fluxes above a deciduous forest in the Midwestern USA. Abstract fra American Geophysical Union Fall Meeting 2013, San Francisco, USA.
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keywords = "atmosphere-biosphere exchange, fluxes, nitrogen, gas-particle partitioning, forest, relaxed eddy accummulation, eddy covariance",
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Hansen, K, Sørensen, LL, Hornsby, KE, Boegh, E & Pryor, SC 2013, 'Influence of gas-particle partitioning on ammonia and nitric acid fluxes above a deciduous forest in the Midwestern USA' American Geophysical Union Fall Meeting 2013, San Francisco, USA, 09/12/2013 - 13/12/2013, .

Influence of gas-particle partitioning on ammonia and nitric acid fluxes above a deciduous forest in the Midwestern USA. / Hansen, Kristina; Sørensen, Lise Lotte; Hornsby, Karen E.; Boegh, Eva; Pryor, Sara C.

2013. Abstract fra American Geophysical Union Fall Meeting 2013, San Francisco, USA.

Publikation: KonferencebidragKonferenceabstrakt til konferenceForskning

TY - ABST

T1 - Influence of gas-particle partitioning on ammonia and nitric acid fluxes above a deciduous forest in the Midwestern USA

AU - Hansen, Kristina

AU - Sørensen, Lise Lotte

AU - Hornsby, Karen E.

AU - Boegh, Eva

AU - Pryor, Sara C.

PY - 2013

Y1 - 2013

N2 - Quantifying the atmosphere-biosphere exchange of reactive nitrogen gasses (including ammonia (NH3) and nitric acid (HNO3)) is crucial to assessing the impact of anthropogenic activities on natural and semi-natural ecosystems. However, measuring the deposition of reactive nitrogen is challenging due to bi-directionality of the flux, and the dynamics of the chemical gas/aerosol equilibrium of NH3 and HNO3 (or other atmospheric acids) with aerosol-phase ammonium (NH4+) and nitrate (NO3-). NH3 and HNO3 are both very reactive and typically exhibit higher deposition velocities than aerosol NH4+. Therefore, the phase partitioning between gas and aerosol phases can have a significant effect on local budgets and atmospheric transport distances (Nemitz et al., Atmos. Chem. Phys., 2004). In this study, fluxes of NH3, HNO3 and carbon dioxide (CO2) along with size-resolved N-aerosol concentrations are measured above the deciduous forest, Morgan Monroe State Forest (MMSF) in south-central Indiana (39°53’N, 86°25’W) during a field campaign. Two relaxed eddy accumulation (REA) systems are used to measure fluxes and concentrations of NH3 and HNO3 at 44 m. The NH3 REA system operates based on wet effluent diffusion denuders with detection by florescence and half-hourly flux measurements are calculated. HNO3 REA system is based on gas capture on sodium chloride (NaCl) coated denuders with subsequent analysis by ion-chromatography, and the resulting fluxes have a resolution of 3-4 hours. CO2 fluxes are measured by eddy covariance using a closed-path Licor LI-7500, while two MSP MOUDI-110 impactors are used to measure the 24-hourly average inorganic and 48 hourly averaged organic ion concentrations in 11 size bins, respectively, just above the canopy level (28 m). The results of this field campaign are used to quantify the fluxes of NH3, HNO3, CO2 to/from the forest during the transition towards senescence, and to investigate process-level controls (e.g. the role of phase partitioning) on the exchange of reactive nitrogen between the forest and the atmosphere.

AB - Quantifying the atmosphere-biosphere exchange of reactive nitrogen gasses (including ammonia (NH3) and nitric acid (HNO3)) is crucial to assessing the impact of anthropogenic activities on natural and semi-natural ecosystems. However, measuring the deposition of reactive nitrogen is challenging due to bi-directionality of the flux, and the dynamics of the chemical gas/aerosol equilibrium of NH3 and HNO3 (or other atmospheric acids) with aerosol-phase ammonium (NH4+) and nitrate (NO3-). NH3 and HNO3 are both very reactive and typically exhibit higher deposition velocities than aerosol NH4+. Therefore, the phase partitioning between gas and aerosol phases can have a significant effect on local budgets and atmospheric transport distances (Nemitz et al., Atmos. Chem. Phys., 2004). In this study, fluxes of NH3, HNO3 and carbon dioxide (CO2) along with size-resolved N-aerosol concentrations are measured above the deciduous forest, Morgan Monroe State Forest (MMSF) in south-central Indiana (39°53’N, 86°25’W) during a field campaign. Two relaxed eddy accumulation (REA) systems are used to measure fluxes and concentrations of NH3 and HNO3 at 44 m. The NH3 REA system operates based on wet effluent diffusion denuders with detection by florescence and half-hourly flux measurements are calculated. HNO3 REA system is based on gas capture on sodium chloride (NaCl) coated denuders with subsequent analysis by ion-chromatography, and the resulting fluxes have a resolution of 3-4 hours. CO2 fluxes are measured by eddy covariance using a closed-path Licor LI-7500, while two MSP MOUDI-110 impactors are used to measure the 24-hourly average inorganic and 48 hourly averaged organic ion concentrations in 11 size bins, respectively, just above the canopy level (28 m). The results of this field campaign are used to quantify the fluxes of NH3, HNO3, CO2 to/from the forest during the transition towards senescence, and to investigate process-level controls (e.g. the role of phase partitioning) on the exchange of reactive nitrogen between the forest and the atmosphere.

KW - atmosphere-biosphere exchange

KW - fluxes

KW - nitrogen

KW - gas-particle partitioning

KW - forest

KW - relaxed eddy accummulation

KW - eddy covariance

M3 - Conference abstract for conference

ER -

Hansen K, Sørensen LL, Hornsby KE, Boegh E, Pryor SC. Influence of gas-particle partitioning on ammonia and nitric acid fluxes above a deciduous forest in the Midwestern USA. 2013. Abstract fra American Geophysical Union Fall Meeting 2013, San Francisco, USA.